长江口溶解氧赤潮预报简易模式
The simple model of dissolved oxygen about red tide forecast in the Changjiang Estuary
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摘要: 在海洋浮游生物中,有很多单细胞微小生物,由于异常地急剧繁殖,并高度密集在一起,从而引起海水变色的现象,称谓“赤潮”.目前,普遍认为赤潮的发生与海水中磷、氮等营养盐、铁、锰等微量元素以及某些有机化合物的大量增加有关[l];另外,还与水体的停滞和气象条件密切联系[2,3].赤潮的发生意味着生态平衡的破坏.
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Key words:
- Red tide /
- dissolved oxygen /
- forecast
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Wang Zhengfang, Zhang Qing, Gong Min. The effects of nitrogen, phosphorus, vitamins and trace metals on the growth of the red tide organism prorocentrum micans. Chin J Oceanol Limmol, 1995, 13(4):338～342 Wang Zhengfang, Zhang Qing, Gong Min. The most suitable initial density of prorocentrum micans and its relationship with temperature. Marine Environment Science, 1993, 12(2):44～47 Zhang Qing, Wang Zhengfang, Gong Min. The preliminary study on the red tide around the Beiji Islands in China. In:David Hopley, Wang Ying, ed. Proceedings of the 1993 Pacon Symposium. James Cook University of North Queensland, Australia, 1993. 421～429 Hallegraeff G M. CSIRO Marine Laboratories Report. 1987. 187 Hallegraeff G M. Gymnodinium catenayum Bloom and shellfish toxicity in Southern Tasmania. Australia. Red Tides. 77 王正方,张庆,吕海燕温度、盐度、pH和光照强度对海洋原甲藻的影响.海洋与湖沼(待刊) 国家海洋局.海洋调查规范.北京:海洋出版社,1975 国家海洋局.海洋监测规范.北京:海洋出版社,1989 -
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